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461.
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Arthur J. Miller Fei Chai Sanae Chiba John R. Moisan Douglas J. Neilson 《Journal of Oceanography》2004,60(1):163-188
Decadal-scale climate variations in the Pacific Ocean wield a strong influence on the oceanic ecosystem. Two dominant patterns
of large-scale SST variability and one dominant pattern of large-scale thermocline variability can be explained as a forced
oceanic response to large-scale changes in the Aleutian Low. The physical mechanisms that generate this decadal variability
are still unclear, but stochastic atmospheric forcing of the ocean combined with atmospheric teleconnections from the tropics
to the midlatitudes and some weak ocean-atmosphere feedbacks processes are the most plausible explanation. These observed
physical variations organize the oceanic ecosystem response through large-scale basin-wide forcings that exert distinct local
influences through many different processes. The regional ecosystem impacts of these local processes are discussed for the
Tropical Pacific, the Central North Pacific, the Kuroshio-Oyashio Extension, the Bering Sea, the Gulf of Alaska, and the California
Current System regions in the context of the observed decadal climate variability. The physical ocean-atmosphere system and
the oceanic ecosystem interact through many different processes. These include physical forcing of the ecosystem by changes
in solar fluxes, ocean temperature, horizontal current advection, vertical mixing and upwelling, freshwater fluxes, and sea
ice. These also include oceanic ecosystem forcing of the climate by attenuation of solar energy by phytoplankton absorption
and atmospheric aerosol production by phytoplankton DMS fluxes. A more complete understanding of the complicated feedback
processes controlling decadal variability, ocean ecosystems, and biogeochemical cycling requires a concerted and organized
long-term observational and modeling effort.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
464.
前期蛋白质质谱分析发现,松江鲈(Trachidermus fasciatus Heckel)经鳗弧菌(Vibrio anguillarum)刺激后,其皮肤黏液中的肌酸激酶(creatine kinase,CK)的表达明显上调。目前,肌酸激酶在鱼类中的功能研究尚未深入开展。本文利用RACE技术克隆获得了松江鲈CK基因的全长cDNA序列(命名为TfM-CK)。TfM-CK基因的cDNA全长为1 474 bp,开放阅读框为1 146 bp,编码381个氨基酸。序列比对分析显示,TfM-CK序列高度保守。实时荧光定量PCR显示,TfM-CK mRNA广泛表达于松江鲈各组织,在肌肉中的相对表达量最高,其次为血液。鳗弧菌刺激后,TfM-CK mRNA在肌肉、皮肤、脾脏和头肾中均上调表达。其中,脾脏中的表达量高达对照组的900多倍。原核重组表达纯化的TfM-CK (rTfM-CK)蛋白酶活测定实验结果显示,重组蛋白的酶活为22.0 U/mg。rTfM-CK对鳗弧菌、大肠杆菌(Escherichia coli)、巨大芽孢杆菌(Bacillus megaterium)和金黄色葡萄球菌(Staphylococcus aureus)有较强的凝集作用。由以上实验结果推测,TfM-CK可能通过细菌凝集作用参与到了松江鲈抵抗病原菌的先天免疫防御过程中。本研究为认识鱼类肌酸激酶的功能及其在病原菌防御过程中的分子免疫机制机制提供了参考。 相似文献
465.
Zenghong Liu Xiaogang Xing Zhaohui Chen Shaolei Lu Xiaofen Wu Hong Li Chunling Zhang Lijing Cheng Zhaoqin Li Chaohui Sun Jianping Xu Dake Chen Fei Chai 《海洋学报(英文版)》2023,42(2):1-2
The international Argo program, a global observational array of nearly 4 000 autonomous profiling floats initiated in the late 1990s, which measures the water temperature and salinity of the upper 2 000 m of the global ocean, has revolutionized oceanography. It has been recognized one of the most successful ocean observation systems in the world. Today, the proposed decade action “OneArgo” for building an integrated global, full-depth, and multidisciplinary ocean observing array for beyond 2020 ... 相似文献
466.
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???????С??????????????????????????????????????С???????????????????????????????μ?ITRF2005???????????????????????????????????????????e???????????????????????????????????????????????£???NNR-NUVEL1A????????????н????????????????С???????????????????????????????????? 相似文献
467.
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469.
Changes in reference evapotranspiration over China during 1960–2012: Attributions and relationships with atmospheric circulation
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This study investigates reference evapotranspiration (ET0) trends in China from 1960 to 2012 based on the Penman–Monteith equation and gridded meteorological measurements. Under the combined impacts of factors influencing ET0 (i.e., net radiation [RN], mean temperature [TAVE], vapour pressure deficit [VPD], and wind speed [WND]), both seasonal and annual ET0 for the whole China and more than half of the grids decreased over the past 53 years. The attribution analyses suggest that for the whole China, the WND is responsible for annual and seasonal ET0 decreases (excluding summer, where RN is responsible). Across China, the annual cause of WND with the largest spatial extent (43.1% of grids) mainly derives from north of the Changjiang River Basin (CJRB), whereas VPD (RN) as a cause is dispersedly distributed (within and to the south of the CJRB). In summer, RN is dominant in more than half of the grids, but the dominance of VPD and WND accounts for approximately 90% of grids during the remaining seasons. Finally, the correlation coefficients between ET0 and the Atlantic Oscillation (AO), North AO, Indian Ocean Dipole (IOD), Pacific Decadal Oscillation (PDO), and El Niño Southern Oscillation (ENSO) indices with different lead times are calculated. For the whole China, annual and seasonal ET0 always significantly correlate with these indices (excluding the IOD) but with varied lead times. Additionally, near half of the grids show significant and maximum (i.e., the largest one between ET0 and a certain index with a lead time of 0–3 seasons) correlation coefficients of ET0 with PDO in spring and summer, ENSO in autumn, and AO in winter. This study is not only significant for understanding ET0 changes, but it also provides preliminary and fundamental reference information for ET0 prediction. 相似文献
470.
雷电灾害风险评估中损失量的量化分析 总被引:1,自引:0,他引:1
为了更好地做好雷电灾害风险评估,减少雷电带来的损失风险,提出了对雷电灾害风险评估标准中损失量的量化方法。一种方法是基于年雷暴日的量化,另一种方法是利用闪电定位资料,采用了多元回归分析对损失量进行量化,回归试验结果表明:F分布高度显著,相关系数平方可达0.7569。后一种量化方法比前一种量化方法造成的相对误差更小,因此利用年雷暴日量化分析仍存在不足,而基于闪电资料的量化分析更能科学地量化损失量,进而为精细化的雷电灾害风险评估提供科学的参考依据。 相似文献